#------------------------------------------------------------------------------ #$Date: 2016-02-16 14:49:47 +0200 (Tue, 16 Feb 2016) $ #$Revision: 176465 $ #$URL: file:///home/coder/svn-repositories/cod/cif/9/00/94/9009455.cif $ #------------------------------------------------------------------------------ # # This file is available in the Crystallography Open Database (COD), # http://www.crystallography.net/. The original data for this entry # were provided the American Mineralogist Crystal Structure Database, # http://rruff.geo.arizona.edu/AMS/amcsd.php # # The file may be used within the scientific community so long as # proper attribution is given to the journal article from which the # data were obtained. # data_9009455 loop_ _publ_author_name 'Finney, J. J.' 'Graeber, E. J.' 'Rosenzweig, A.' 'Hamilton, R. D.' _publ_section_title ; The structure of chloroxiphite, Pb3CuO2(OH)2Cl2 Locality: Mendip Hills, Somerset, England ; _journal_name_full 'Mineralogical Magazine' _journal_page_first 357 _journal_page_last 361 _journal_paper_doi 10.1180/minmag.1977.041.319.07 _journal_volume 41 _journal_year 1977 _chemical_formula_sum 'Cl2 Cu H2 O4 Pb3' _chemical_name_mineral Chloroxiphite _space_group_IT_number 11 _symmetry_space_group_name_Hall '-P 2yb' _symmetry_space_group_name_H-M 'P 1 21/m 1' _cell_angle_alpha 90 _cell_angle_beta 97.79 _cell_angle_gamma 90 _cell_length_a 10.458 _cell_length_b 5.750 _cell_length_c 6.693 _cell_volume 398.759 _exptl_crystal_density_diffrn 6.847 _cod_original_formula_sum 'Pb3 Cu O4 Cl2 H2' _cod_database_code 9009455 loop_ _symmetry_equiv_pos_as_xyz x,y,z x,1/2-y,z -x,1/2+y,-z -x,-y,-z loop_ _atom_site_label _atom_site_fract_x _atom_site_fract_y _atom_site_fract_z _atom_site_U_iso_or_equiv Pb1 0.21670 0.25000 0.46060 0.01811 Pb2 0.55020 0.25000 0.34320 0.01697 Pb3 0.67410 0.25000 0.86730 0.01710 Cu 0.00000 0.00000 0.00000 0.02039 O1 0.36600 0.00000 0.38600 0.01672 O-H1 0.90700 0.25000 0.83200 0.01735 O-H2 0.12600 0.25000 0.08600 0.02178 Cl1 0.37800 0.25000 0.86800 0.02128 Cl2 0.88600 0.25000 0.32100 0.03090